“…The formation and instability of current sheets with stretched magnetic field lines is a common problem in both magnetotail and solar physics (Reeves et al., 2008; Terasawa et al., 2000). In the latter case magnetic reconnection is believed to explain charged particle acceleration and magnetic field energy release in eruptive flares (the so called standard CSHKP model, see Carmichael, 1964; Hirayama, 1974; Kopp & Pneuman, 1976; Sturrock, 1966), non‐eruptive events (including, e.g., coalescence of magnetic loops, see Sakai & de Jager, 1996), streamers (e.g., Edmondson & Lynch, 2017; Riley & Luhmann, 2012; Réville et al., 2020), and solar wind current sheets (Gosling, 2012; Phan et al., 2006). In contrast to the magnetotail investigations, mostly focused on the stabilization of the tearing mode by field, the theory of tearing instability for solar applications is dominated by models of resistive tearing mode in sheets (e.g., Del Sarto et al., 2016; Dobrowolny et al., 1983; Loureiro et al., 2012; Ofman et al., 1991; Tenerani et al., 2015).…”